Viscoplastic self‐consistent and equilibrium‐based modeling of olivine lattice preferred orientations: Implications for the upper mantle seismic anisotropy

By A. Tommasi, David Mainprice, G. Canova, Y. Chastel. 2000

381 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/f3de5d760dd6dc88835b00160767e1ff5cd3aaad

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geophysics

Citations in the corpus

Timescales for the evolution of seismic anisotropy in mantle flow (2001, background): “Modeling of plastic deformation in olivine polycrystals has provided important insight into the link between seismic anisotropy and mantle flow [Wenk et al., 1991; Ribe and Yu, 1991; Chastel et al., 1993; Tommasi et al., 2000].”
Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions (2009, methodology): “Various other approaches to model directly fabric development using schemes such as D-Rex (Kaminski et al. 2004) or viscoplastic self-consistent modeling (e.g., Tommasi et al. 2000) have also been implemented (see, e.g., Lev and Hager 2008a).”
Statistical properties of seismic anisotropy predicted by upper mantle geodynamic models (2006, positive): “This finding is consistent with earlier work in two dimensions [Tommasi, 1998; Tommasi et al., 2000; Blackman et al., 2002] and substantiates interpretation of seismic anisotropy using global flow models which were based on instantaneous strain rates [Gaboret et al.”
Organized melt, seismic anisotropy, and plate boundary lubrication (2010, background): “The implication is that anisotropy develops quickly and then saturates with increasing melt segregation, in similar manner to LPO [Tommasi et al., 2000].”
A kinematic model for recrystallization and texture development in olivine polycrystals (2001, background): “This secondary peak, which is also predicted by plastic models without dynamic recrystallization [12], corresponds to hard grains with low dislocation densities that have not yet been consumed by GBM.”
Effect of water and stress on the lattice-preferred orientation of olivine (2006, background): “, 2005), some deep sheared lherzolite xenoliths from kimberlite magmas (Lori Kennedy, private communication 2001), and other peridotites studied by the following authors (e.g., Mercier, 1977; Krull and Voll, 1978; Cordellier et al., 1981; Shuguang and Li, 1998; Tommasi et al., 2000; Pennock et al., ”
Descriptive tools for the analysis of texture projects with large datasets using MTEX: strength, symmetry and components (2014, methodology): “VPSC modelling is now well established as robust method for studing CPO development in minerals undergoing plastic deformtion for all types of strain histories (e.g. Tommasi et al. 2000; Bascou et al. 2002; Ulrich & Mainprice 2005).”
Radial seismic anisotropy as a constraint for upper mantle rheology (2007, background): “Regional models interpreting LPO texture exist (e.g. Chastel et al., 1993; Tommasi et al., 2000; Blackman and Kendall, 2002; Wenk et al., 2006), and LPO formation has also been tested in global flow,where it was found that the heterogeneity of the synthetic LPO textures matches that of mantle…”
Comparison of azimuthal seismic anisotropy from surface waves and finite strain from global mantle-circulation models (2003, background): “…the finite strain ellipsoid (FSE), or, alternatively, the orientation of the shear plane, will vary and may depend on the exact strain history, temperature, mineral assemblage of the rock and possibly other factors (e.g. Savage 1999; Tommasi et al. 2000; Blackman et al. 2002; Kaminski & Ribe 2002).”